Research Article

Improving yield and water use efficiency of apple trees through intercrop-mulch of crown vetch Coronilla varia L.) combined with different fertilizer treatments in the Loess Plateau

Wei Zheng

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Yonggang Li

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Qingli Gong

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Haoqing Zhang

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Zhiyuan Zhao

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Zhaoxia Zheng

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Bingnian Zhai

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Zhaohui Wang

Northwest A&F University, College of Resources and Environment, Key Laboratory of Plant Nutrition and the Agri-environment
in Northwest China, Ministry of Agriculture, Yangling, Shaanxi 712100, China

Abstract

Improving water use efficiency (WUE) and soil fertility is relevant for apple production in drylands. The effects of intercrop-mulch
(IM) of crown vetch (Coronilla varia L.) combined with different fertilizer treatments on WUE of apple trees and soil fertility of apple orchards were assessed
over three years (2011, 2013 and 2014). A split-plot design was adopted, in which the main treatments were IM and no intercrop-mulch
(NIM). Five sub-treatments were established: no fertilization (CK); nitrogen and phosphorus fertilizer (NP); manure (M); N,
P and potassium fertilizer (NPK); and NPK fertilizer combined with manure (NPKM). Due to mowing and mulching each month during
July–September, the evapotranspiration for IM was 17.3% lower than that of NIM in the dry year of 2013. Additionally, the
soil water storage of NPKM treatment was higher than that of CK during the experimental period. Thus, single fruit weight
and fruit number per tree increased with IM and NPKM application. Moreover, applying NPKM with IM resulted in the highest
yield (on average of three years), which was 73.25% and 130.51% greater than that of CK in IM and NIM, respectively. The WUE
of NPKM combined with IM was also the highest in 2013 and 2014 (47.69 and 56.95% greater than applying IM alone). In addition,
due to application of IM combined with NPKM, soil organic matter was increased by 25.8% compared with that of CK (in NIM).
Additionally, application of IM combined with NPKM obtained more economic net return, compared to other combinations. Therefore,
applying NPKM with IM is recommended for improving apple production in this rain-fed agricultural area.

China is the biggest apple producing country in the world (Liu Y et al., 2013), with a cultivated area of 2.41 × 106 ha (46% of the world surface devoted to apple) producing 39.68 × 106 t of apples (49% of the world’s total production) in 2013 (http://faostat3.fao.org/home/E). In China, the Loess Plateau is a large area of apple production that represents 28.09 and 25.73% of the country’s apple
cultivation area and total yield, respectively (Yang & Chen, 2013). The apple products of the Loess Plateau area have been exported to more than 30 countries in Europe, North America and
Southeast Asia (Li et al., 2008; Yang & Chen, 2013; Qian et al., 2015). However, the Loess Plateau is also the largest dryland rain-fed agricultural area in China, and water resource deficiencies
seriously restrict apple production (Huang & Gallichand, 2006). In 2010, the apple yield per hectare in the Loess Plateau (with annual mean rainfall and potential evaporation of 200–700
and 763–963 mm, respectively) was 14.22 t/ha, only 47% of that of the Bohai Coastal area (30.15 t/ha) (with annual mean rainfall
and potential evaporation of 550–950 and 450–600 mm, respectively) (Pu et al., 2010; Yang & Chen, 2013; Zhang et al., 2014). Thus, decreasing water loss from evaporation and increasing yield per unit area is a great challenge for improving apple
production of the Loess Plateau.

In the Loess Plateau, almost 70% of rainfall usually occurs from the hot summer to early autumn (July–September), and much
of this is lost through evaporation due to seasonal high temperatures (Ren et al., 2008). Thus, limited annual precipitation and high evaporation in the hot season are the main constraints for apple production.
Additionally, apple trees have more extensive root systems and canopy than annual crops, so apple orchards have higher evapotranspiration
and lower available soil water in comparison with local cereal crops (e.g. winter wheat) (Huang & Gallichand, 2006). Evaporation during hot summers may cause soil moisture deficits of various degrees in apple orchards when precipitation
is limited. Low soil fertility is another constraint. Soil organic matter (SOM) in most apple orchards of the Loess Plateau
is usually in the range of 1.0–1.5% due to the application of inorganic fertilizer without organic inputs, which is much lower
than that of American apple orchards (> 2.0%) (Chen et al., 2014; Zhao & Tong, 2014). The stability of macro-aggregates and moisture retention capacity are also low due to the application of chemical fertilizer
alone (Sarkar et al., 2003). Therefore, development of suitable water management measures and rational fertilization are needed to sustain apple production
in the Loess Plateau.

As a perennial legume, crown vetch (Coronilla varia L.) is a common intercropping plant in apple orchards with many benefits, including controlling weeds, decreasing soil erosion,
fixing atmospheric N2, increasing soil enzyme activities, and improving the soil micro-ecological environment (Jarvis, 1983; Cardina et al., 1986; Qian et al., 2015). However, intercropping of crown vetch might compete with apple trees for water (Li et al., 2014). Mulch application could help to conserve soil water and decrease evaporation (Sauer et al., 1996; Burt et al., 2005; Monzon et al., 2006; Yuan et al., 2009; Ward et al., 2009). Thus, intercrop-mulch (IM), a process involving intercropping with crown vetch at first and then mowing it (the residues
are left on the soil surface as mulch) in the rainy hot season, is recommended. However, the effect of IM on water use efficiency
(WUE) in apple production is unclear, especially with regard to differences in water consumption before and after mulch application.
In addition, although mulch can significantly decrease evaporation, the WUE can still be very low due to a lack of adequate
fertilizer use (Li et al., 2000). Many studies have shown the effects of straw mulch and plastic film or combinations of mulch with varied nitrogen (N) rates
on the WUE of cereal crops (Li et al., 2001; Khurshid et al., 2006; Chen et al., 2015; Li et al., 2015). However, little is known about the effect of applying IM of crown vetch with different kinds of fertilization on the WUE
of apple trees.

Current apple production in the Loess Plateau can be substantially increased by rational water conservation and fertilization
measures. Thus, a field experiment was conducted aiming to: (1) evaluate the combined effects of IM and different kinds of
fertilization on soil water storage, evapotranspiration, yield components, yield, and WUE of apple trees under dryland conditions;
and (2) find the best combination of these strategies for apple production in the rain-fed area of the Loess Plateau.

The experimental site was a typical Loess Plateau area located at the Weibei Dryland Experimental Station of the Northwest
Agriculture and Forestry University (109°56ʹE, 35°21ʹN; altitude of 838 m), Baishui County, Shaanxi Province, China. The soil
of the apple orchard was silt loam (with 8% sand, 67% silt and 25% clay) and classified as Haplustalfs according to USDA system
of soil taxonomy. The topsoil had the following chemical characteristics at the beginning of the experiment: pH 8.3, organic
matter content 13.02 g/kg, total N 1.03 g/kg (Kjeldahl method), available N 24.90 mg/kg (extracted with KCl and quantified
with a flow injection analyzer), Olsen-phosphorus (P) 15.94 mg/kg and available potassium (K) 151.28 mg/kg (extracted by NH4OAc and determined using a flame photometer). The rainfall distribution is dominated by the monsoon climate. In this region,
summer is hot (daily maximum temperatures can reach 39.4 °C in July) and moist, whereas winter and early spring are always
cold (daily minimum temperatures can reach −16.7 °C in January) and dry. In average, total annual radiation for this site
is 5360 MJ/m2 and the number of sun hours is 2477 h. There are usually 171 frost-free days each year. Agriculture in this region is completely
dependent on natural precipitation.

Experimental design and treatments description

Fuji apple trees (Malus pumila Mill.) planted in 2005 on M26 (rootstock) were used as the experimental crop and had a density of 1200 plants/ha. A split-plot
design was adopted, with main plots of IM (with crown vetch) and control (NIM, no crown vetch planted) and sub-plots included
five fertilization treatments: no fertilization, CK; N and P fertilizer (NP); manure (M); N, P and K fertilizer (NPK); and
NPK fertilizer combined with manure (NPKM). Each treatment was replicated three times. Each sub-treatment replicate contained
two rows with 12 apple trees in each row. The surface area of each replicate was about 200 m2. For IM, crown vetch was sown in each inter-row of apple trees (1.6-m-wide strip) in 2008 at a depth of 1.5 cm with a sowing
rate of 6.0 kg/ha. Crown vetch sprouted in late March each year and was mowed (the residues were left on the soil surface
as mulch) in early July, August and September. For NIM, no crown vetch was planted and weeds were controlled by mowing. Urea
(containing 46% N), calcium superphosphate (containing 12% P2O5) and potassium sulfate (containing 50% K2O) were used as N, P and K fertilizers, respectively. The goat manure contained 35.1% dry organic matter, 0.533% N, 0.309%
P2O5 and 0.467% K2O. The fertilizing rates of the sub-treatment groups are shown in Table 1.

Table 1.
Fertilizer rates applied to the different treatments in the intercrop-mulch and no intercrop-mulch.

Precipitation and air temperature during the experimental period

The data were collected during 2011–2014. However, only 2011, 2013 and 2014 data were analyzed due to loss of fruit from hailstones
in 2012. Precipitation (including snow during the winter months) and air temperature were recorded by a weather station placed
at the experimental station and shown in Figs. 1A and 1B. Annual precipitation for 2011, 2013 and 2014 was 767.9, 489.6 and 601.5 mm, respectively. According to the inter-annual
precipitation distribution, 2011 was defined as a wet year, 2013 was a dry year and 2014 was a normal year (Guo et al., 2012). In addition, precipitation during July–September (after mowing) in 2011, 2013 and 2014 was 469, 316.2 and 341.2 mm, respectively,
accounting for 61, 65 and 57% of annual precipitation. In 2013, the annual accumulated temperature was about 4403 °C, which
was 7.73 and 2.02% higher than that of 2011 (4087 °C) and 2014 (4316 °C), respectively.

Soil samples from each treatment (three soil cores per replicate) were collected from 0 to 200 cm deep at 20 cm intervals
using an open-faced bucket probe (5 cm diameter). Soil samples were collected three times per year at a distance of 50 cm
from tree trunks toward the row space, before sprouting of crown vetch (late March), before the first mowing and mulching
of crown vetch (early July) and after apple ripening (late September). However, soil samples were not collected in early July
of 2011 due to lack of manpower. Fresh soil samples were taken to the laboratory to determine their gravimetric water content.
Soil bulk density was measured according to Li R et al. (2013) (Fig. 2). Soil samples from the 0–20 and 20–40 cm soil layers were collected after harvesting in 2014 and used to determine SOM.
Three soil cores were collected in each replicate. Prior to analysis of organic matter, soil samples were air dried and passed
through a 0.25-mm sieve. The SOM content was determined by potassium dichromate oxidation at 170–180 °C, followed by titration
with 0.1 mol/L ferrous sulfate (Bao, 2000).

Evapotranspiration was calculated using the following formula (Qin et al., 2013):

where ET is water consumption in a period; 10∑γi Hi θi is the soil water storage; i is the soil layer; n is the total number of soil layers; γi is the soil bulk density of layer i; Hi is the thickness (cm) of layer i; θi1 and θi2 are gravimetric water contents of layer i at the beginning and end of the measuring period, respectively; and P0 is the precipitation during each measuring period.

Apple fruits were collected from trees in each treatment group at harvest. Nine trees were randomly chosen from each replicate
for investigating the fruit number per tree, fruit weight and yield of each replicate. Yield per tree was measured using a
scale. The apple yield (t/ha) of each replicate was calculated by fruit weight, fruit number/tree, and tree number/ha. WUE
was calculated with the formula WUE = Y / ET, where Y is apple yield.

The total cost and yield return was calculated for three years. Seed and sowing costs include the cost of crown vetch seed
and sowing. Mowing cost was the cost of crown vetch mowing for IM and weed mowing for NIM. Others costs included the cost
of orchard management. All costs were converted from Chinese yuan to Euro (€1 = ¥6.81). Yield return was calculated (¥4 /
kg).

SPSS 19.0 was used to conduct analysis of variance. Two-way ANOVA was used for assessing differences among treatments, sub-treatments
and their interactions. Least significant difference (LSD) was used for mean separation. The figures were constructed using
Sigma Plot 12.0 software.

There were no obvious effects of IM on soil water storage in late March (2013) and late September (2011 and 2013), and significant
effects during other periods in 2011, 2013 and 2014. In addition, fertilization significantly affected soil water storage
each year, and the interaction effect of fertilization and IM on soil water storage in late March was significant (Table 2). Additionally, over the experimental years of 2011, 2013 and 2014, soil water storage decreased with water consumption by
apple trees and crown vetch, and increased at the expansion stage of apple trees in the rainy season (July–September) (Table 3). In IM and NIM treatments, soil water storage of M and NPKM tended to be higher than that of CK, NP and NPK in 2011, 2013
and 2014. The mean soil water storage of IM in late March of 2011 and 2014 was significantly higher than that of NIM with
no difference between IM and NIM in late March of 2013. In early July, mean soil water storage of IM was lower than that of
NIM in 2013, but it was higher than that of NIM in 2014. However, in late September, the difference in mean soil water storage
was significant only in 2014, with that of IM higher than that of NIM.

Table 2.
Analysis of variance of the effects of intercrop-mulch (IM), fertilization, and their interaction on soil water storage and
ET (p-values are shown).

Table 3.
Soil water storage during different periods (late March, early July and late September), ETtot, ETbm and ETmow in 2011, 2013 and 2014.

The effects of IM on ETtot (total evapotranspiration), ETbm (evapotranspiration from late March to early July) and ETmow (evapotranspiration from early July to late September) were prominent, even though there were no effects on ETtot in 2013 and ETmow in 2014. For fertilization, there were significant effects on ETtot each year and ETbm in 2014. The obvious interaction of IM and fertilization on ETtot (in 2011 and 2014) and ETbm (2014) was also obtained (Table 2). Moreover, the ETtot of the M, NPK and NPKM was higher than that of CK and NP, with the ETtot of NPKM being the highest, although not all differences were significant (Table 3). Additionally, the ETbm of NPKM was higher than that of CK under NIM (2013) and IM (2014). However, there were no significant differences between
sub-treatments for ETmow. The mean ETtot of IM in 2014 was significantly higher than that of NIM, with no difference between IM and NIM in 2011 and 2013. Similarly,
before the first mowing and mulching (from late March to early July), the ETbm of IM was higher than that of NIM in both 2013 (dry year) and 2014 (normal year). Three periods of mulching (successive mowing
and mulching once per month from early July to late September) caused the ETmow of IM to decrease by 17.3% in comparison with that of NIM in the hot rainy season of 2013 (dry year), although there were
no significant differences between IM and NIM in 2014 (normal year).

Yield components

There was a significant effect of IM on single fruit weight in 2014 (p < 0.05), and no significant effect in 2011 and 2013. Additionally, the impact of IM on fruit number per tree was significant
only in 2011 and 2013 (p < 0.01); whereas, fertilization markedly affected single fruit weight and fruit number per tree in each year (Table 4). Additionally, there were no significant interactions between IM and fertilization for single fruit weight or fruit number/tree
in 2011, 2013 and 2014. In 2014, the single fruit weight of IM was 8.5% higher than that of NIM, while the fruit number per
tree of IM was 6.2 and 68.9% higher than that of NIM in 2011 and 2013, respectively (Table 5). The mean single fruit weight and fruit number per tree of NPKM treatment under IM were 20.89% and 42.21% higher than those
of CK under IM, respectively; with a similar trend also observed for the NIM treatment (Table 5). Additionally, IM increased single fruit weight in 2014 and fruit number per tree in 2011 and 2013. Thus, applying IM with
NPKM treatment was much more effective than single application of IM, especially in the dry year.

Table 4.
Analysis of variance of the effects of intercrop-mulch (IM), fertilization and their interaction on apple fruit weight, fruit
number per tree, yield, WUEtot (water use efficiency from late March to late Sept ember) and WUEmow (water use efficiency from early July to late September) (p-values are shown).

Table 5.
Yield components of apple for all fertilizer treatments under intercrop-mulch (IM) and no intercrop-mulch (NIM).

Apple yield and WUE

IM and fertilization affected apple yield and WUE from late March to late September (WUEtot) and WUE from early July to late September (WUEmow), because the single fruit weight or single fruit number per tree was affected, although the effect of IM on WUEtot was not significant in 2014 (Table 4). The apple yield of IM was 6.5%, 69.5% and 30.3% higher than that of NIM in 2011, 2013 and 2014, respectively. Thus, the
WUEtot of IM was 73.3% higher than that of NIM in 2013 (dry year), although this trend was not observed in years with enough precipitation
(2011 and 2014). Especially after applying mulch in the rainy season, the WUEmow of IM was increased by 100.4% and 28.1% in 2013 and 2014, respectively, in comparison with that of NIM (Table 6). In addition, the trees subjected to the NPK and NPKM treatments produced higher apple yield than those subjected to the
other fertilization treatments, with the highest yield in each year for the NPKM treatment, although differences in the yields
of M, NPK, and NPKM under IM in 2013 were not significant. The WUEtot of NPKM under IM was significantly higher than that of CK under IM. The WUEtot of NIM also followed the same trend. In addition, the mean WUEmow of NPKM under IM was the highest (75.86% higher than that of CK under IM).

Table 6.
Yield, WUEtot (WUE from late March to late September) and WUEmow (WUE from early July to late September) of apple under IM (intercrop-mulch) and NIM (no intercrop-mulch) for different fertilizers.

SOM content

Soil organic matter was significantly increased by seven years of IM application (2008–2014) (Table 7). In comparison with CK under NIM, the SOM (0–20 cm) of CK under IM was increased by 11.8%; the M and NPKM treatments under
IM resulted in the highest SOM. Compared with CK under IM, the SOM (0–20 cm) of M and NPKM under IM was 19.1% and 15.8% higher,
respectively, and correspondingly 19.5% and 20.3% higher for SOM at 20–40 cm depth. These results suggest that the applications
of IM and manure increased SOM.

The average net return of IM was 31.48% higher than that of NIM (Table 8). In addition, the cost of IM was only €110.7 higher than that of NIM. The NPKM treatment had the highest net return of any
treatment for both IM and NIM.

Table 8.
Production cost and economic benefit of the different treatments (the cost and economic benefit were the total for three years)
(EUR/ha) [1].

About 70% of yearly precipitation usually occurs from the middle of the hot summer to early autumn (July–September) in rain-fed
dryland apple orchards in the study area; thus, this period has sufficient rainwater resources. However, the high temperature
in this period induces a high amount of water evaporation. Additionally, this period coincides with the fruit expansion stage
when adequate soil water is imperative. Therefore, decreasing ineffective water evaporation during this period could improve
apple tree growth, yield, and WUE.

In the present study, under IM with crown vetch, single fruit weight and fruit number per tree were significantly increased
in comparison with the NIM treatment (Table 5). The apple yield and WUE under IM increased by 27.4% and 14.6% during the three years studied, respectively; particularly
in the dry year, they significantly increased by 69.5% and 73.3%, respectively, although the increase in WUE was not obvious
due to a lack of water stress in 2011 and 2014, during which there was enough precipitation. The yield and WUE of IM were
increased due to the application of mulch three times during June–September, which decreased evaporation from topsoil and
improved soil water storage. The water stored through mulch application surpassed or at least compensated for the water consumed
in crown vetch growth. However, Du et al. (2015) found that apricot yield decreased due to water competition between erect milk vetch and apricot in an intercrop-mulching
system, even though the mulch was applied after mowing, probably because mulch was applied too late (in autumn) to be effective
for seasonal fruit growth as apricots had already ripened (in July). In the present study, successive monthly mowing and mulching
during July–September would substantially restrain the competition capacity of crown vetch and decrease water evaporation
in the hot rainy season. Especially in the dry year, mowing and mulching significantly decreased ETmow by 17.3% in comparison with that of CK (Table 3). Thus, more water was stored for apple tree growth and WUEmow in the rainy hot summer was significantly increased (Table 6). Additionally, although growth of crown vetch would consume some soil water before mowing (from late March to early July)
and so compete for soil water with apple trees and increase ETtot, the apple yield still increased. A possible explanation for this observation was the adaptive spatial complementarity of
the two root systems, which may have prevented water competition (Fetene et al., 2003; Morlat & Jacquet, 2003). Monteiro & Lopes (2007) found that the water depletion that was observed in the sward treatments at bloom time may have induced death of vine roots
in the upper layers and development of a deeper root system to explore deeper layers. Li et al. (2011) also reported that apple roots extended more into deep soil layers, while fine roots extended more deeply into soil layers
than thick roots did, and white clover fine roots extended more into surface soil layers in the apple-white clover intercropping
system. After mowing and mulching from July-September, IM treatment can result in more water storage for fruit growth in comparison
with NIM. Taken together, these results indicate that IM increased apple yield, showing that there is great potential for
decreasing evaporation and increasing apple yield and WUE through IM with crown vetch if crown vetch is well managed and competition
with apple trees prevented.

Although IM of crown vetch can decrease evaporation and store more water for transpiration of apple trees, adequate fertilization
is still needed in combination with IM to increase WUE. In our experiment, soil fertility was improved after applying IM with
NPKM for seven years. The SOM of NPKM (with IM) at depths of 0–20 and 20–40 cm was increased by 15.8 and 20.3% in comparison
with that of CK under IM, respectively (Table 7). Thus, single fruit weight and fruit number per tree were obviously increased. Therefore, apple yield for NPKM (with IM)
was increased by an average of 73.25% in the three studied years; the WUEmow of NPKM (with IM) was also significantly increased by 75.86% in comparison with that of CK (with IM). These results suggest
that NPKM fertilization supplies sufficient available nutrients for tree growth and improves soil fertility in the long term,
in comparison with NPK fertilization (Lönhárd-Bory & Németh, 1990; Zhao et al., 2014). As a result, we suspect that apple trees subjected to NPKM treatment likely had larger canopies (Li TT et al., 2013), while soil water, which was conserved by mulch, was efficiently used for transpiration, so apple yield and WUEmow increased. Previous research had reported that intercropping might decrease yields because of nutrient competition (Du et al., 2015). In our experiment, NPKM treatment improved soil fertility more than other fertilization treatments. Therefore, NPKM treatment
was more effective than other treatments as a means of mitigating nutrient competition between crown vetch and apple trees.
In addition, due to the manure addition, which could improve the mean weight diameter of aggregates, total porosity, and water
holding capacity (Karami et al., 2012; Liu CA et al., 2013), NPKM fertilization could induce water storage more effectively than chemical fertilizer alone, mitigating water competition
between crown vetch and trees. As a result, NPKM fertilization could greatly compensate for nutrient deficiency with IM and
applying the two together could result in greater apple yields compared to applying IM with other fertilizers, benefiting
farmers (Table 8). In the Loess Plateau, farmers always apply plastic film and straw mulch to decrease the evaporation. However, plastic film
does not increase the abundance of soil nutrients and has negative environmental impacts, and both plastic film and straw
mulch impose transportation expenses and other costs each year. As a perennial legume, crown vetch can live for several years
if well managed and sprout in late March each year after being sown in the first year, and it can form root nodules, control
weeds, prevent soil erosion, and improve soil fertility (Wheeler, 1974; Symstad, 2004). As a legume, crown vetch can mitigate nitrogen competition due to its ability to fix atmospheric N2 via root nodules, compared to other non-legume species, and other similar studies found that nitrogen competition was mitigated
by legume grass cover systems (King & Berry, 2005; Messiga et al., 2015). In our experiment, the total net return (for three years) of IM was 31.5% higher than that of NIM, and that of IM combined
with NPKM was 72.35% higher than that of IM alone. All of these reasons indicate that IM of crown vetch combined with NPKM
is a good practice for apple production, although it may compete for soil water with apple trees before the first mowing and
mulching.

In summary, applying IM conserved more soil water in the hot rainy season for transpiration during the fruit expansion stage
of apple trees, particularly in the dry year, although the effect was not obvious when enough precipitation prevented water
stress. Thus, single fruit weight and fruit number per tree increased, as well as apple yield and WUE. Additionally, in comparison
with other fertilization treatments, the water and nutrients consumed by crown vetch were more effectively compensated by
NPKM application. Hence, IM with NPKM resulted in the highest yield and WUE of the tested treatments. For these reasons, and
considering agricultural, soil and economic factors, IM combined with NPKM is expected to be a beneficial practice for farmers
engaged in apple production in the Loess Plateau.

Huang MB, Gallichand J, 2006. Use of the SHAW model to assess soil water recovery after apple trees in the gully region of
the Loess Plateau, China. Agric Water Manage 85: 67-76. https://doi.org/10.1016/j.agwat.2006.03.009

Li TC, Li HK, Guo H, Du YF, Wang HT, 2014. Moisture characteristics of different herbages on soil water in apple orchard in
the area of Weibei Plateau in dry season. Research of Soil and Water Conservation 21: 29-38. [In Chinese].